Bauxite

Reddish-brown bauxite
Bauxite with US penny for comparison
QEMSCAN mineral maps of bauxite ore-forming pisoliths

Bauxite (/ˈbɔːkst/ ) is a sedimentary rock with a relatively high aluminium content. It is the world's main source of aluminium and gallium. Bauxite consists mostly of the aluminium minerals gibbsite (Al(OH)3), boehmite (γ-AlO(OH)), and diaspore (α-AlO(OH)), mixed with the two iron oxides goethite (FeO(OH)) and haematite (Fe2O3), the aluminium clay mineral kaolinite (Al2Si2O5(OH)4) and small amounts of anatase (TiO2) and ilmenite (FeTiO3 or FeO·TiO2).[1][2] Bauxite appears dull in luster and is reddish-brown, white, or tan.[3]

In 1821, the French geologist Pierre Berthier discovered bauxite near the village of Les Baux in Provence, southern France.[4][5]

  1. ^ Geological Survey (U.S.) (1986). Geological Survey Professional Paper. U.S. Government Printing Office. p. 2-PA20.
  2. ^ "The Clay Minerals Society Glossary for Clay Science Project". Archived from the original on April 16, 2016.
  3. ^ "Aluminum". Minerals Education Coalition.
  4. ^ P. Berthier (1821) "Analyse de l'alumine hydratée des Beaux, département des Bouches-du-Rhóne" (Analysis of hydrated alumina from Les Beaux, department of the Mouths-of-the-Rhone), Annales des mines, 1st series, 6 : 531–534. Notes:
  5. ^ Burgess, N. (October 26, 2015). "March 23, 1821: Bauxite Discovered". Earth. Retrieved July 31, 2021.

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